P. Zhong et al., TRANSIENT OSCILLATION OF CAVITATION BUBBLES NEAR STONE SURFACE DURINGELECTROHYDRAULIC LITHOTRIPSY, Journal of endourology, 11(1), 1997, pp. 55-61
Using high-speed photography and acoustic emission measurements, we st
udied the dynamics of a transient cavitation bubble near a stone surfa
ce and the concomitant shockwaves generated during electrohydraulic li
thotripsy (EHL), At each spark discharge, a vapor plasma and subsequen
tly a cavitation bubble oscillating around the tip of an EHL probe are
produced, Simultaneously, three distinctive shockwave pulses are gene
rated, The first shockwave is produced by the rapid expansion of the v
apor plasma, while the second and third waves are produced by rebounds
of the cavitation bubble, Depending on the proximity of the probe to
the stone surface, the collapse of the cavitation bubble may be symmet
ric, resulting in a strong shockwave emission; or asymmetric, leading
to the formation of a liquid jet, For the Nortech AUTOLITHTM lithotrip
ter with a 1.9F probe that was used in this study, maximum shockwave e
mission is produced when the probe is about 1 mm from the stone surfac
e, whereas the maximum jet velocity is produced when the probe tip is
at distance equivalent to the maximum bubble radius of about 3 mm, The
se findings are consistent with clinical experience, which suggests th
at for optimal treatment results, the EHL probe should be placed close
to the stone surface.